Cohiba Minerals Limited provided the following update in relation to the Warriner Creek Project. The Warriner Creek Project comprises 2 tenements under exploration licence to TDG, EL 6324 (Areas A and B) and EL 6533, which cover a combined area of 346 km2 over strategic IOCG targets in the Gawler Craton. The Warriner Creek prospects are located in the high metamorphic temperature Mount Woods Domain which is a sparsely outcropping domain in the far north Gawler Craton.

IOCG (iron ore - copper - gold) style deposits have been discovered in this domain, such as Peak Iron's Peculiar Knob and Cu River Mining's Cairn Hill. Cairn Hill was mined as a magnetite iron ore deposit with accessory copper and gold, and Peculiar Knob is mined as a hematite iron ore deposit. Immediately south of the Mount Woods Domain and 20km south ofWarriner Creek West lies Oz Mineral's Prominent Hill copper-gold mine.

Exploration by Cohiba was focused on IOCG and related skarn style deposits, with a secondary focus on any REE (rare earth element) potential in the area. WARRINER CREEK EAST: Targeting at Warriner Creek East focussed on an isolated slightly offset magnetic and gravity high, with a scale consistent with a Carrapateena sized geophysical anomaly. Drilling intersected complexly deformed high temperature meta-sediments, and into mafic-intermediate diorite with strong magnetite intrusive at depth.

The strongly magnetic diorite is presumed to be the cause of the magnetic geophysical signature. The fact that the gravity anomaly is offset from the magnetic signature presents the possibility that another dense body is the cause of the gravity anomaly. Brecciation and alteration of IOCG style was not observed.

WARRINER CREEK WEST: Warriner Creek West is adjacent to the Peak Iron IOCG related iron ore mine, and near to Oz Minerals Prominent Hill copper-gold mine. Targeting focused on a shallow magnetic ridge running approximately east- west through the tenement. Drilling intersected high temperature meta-sediments and meta-granites.

A south dipping contact from sandy dominant to muddy dominant meta-sediments exhibited a minor mafic dyke in CHK22WCW01 and a healed breccia in CHK22WCW02 with minor magnetite alteration, and trace chalcopyrite and pyrite. It is believed that this contact and mafic intrusions along the contact are the cause of the magnetic anomaly. WARRINER CREEK EAST DRILLING RESULTS: Drill hole CHK22WCE01 returned some anomalous rare earth element (REE) results which were converted to total rare earth oxides (TREO).

The following results occurred: 2m @ 1,532ppm TREO from 504 - 506m. 15m @ 853ppm TREO from 597 - 612 m including 2m @ 1,014ppm TREO from 604m. WARRINER CREEK WEST DRILLING RESULTS: Drill hole CHK22WCW01 returned one low grade copper result and one anomalous rare earth element (REE) result which was converted to total rare earth oxides (TREO).

The following results occurred: 1m @ 0.93% Cu from 128 - 129m. 2m @ 1,053ppm TREO from 139 - 141m.